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Preska on ) (va) (Entered: )ĭECLARATION of Marjorie J. Defendant Manuel may serve the same or additional requests for admission on the Commission and renew his motion after the Commission responds.

The Pallas Defendants shall respond to the four interrogatories that are the subject of the Commission's motion by no later than Friday, October 8, 2021. Manuel is permitted to depose Enright about facts he perceived when meeting with witnesses and corresponding with witnesses and/ or their counsel, in the course of the Commission's investigation. The Deposition Protective Order Motion is DENIED. By no later than Friday, October 1, 2021, Salviola and Pallas shall: (a) Specifically identify which portions of the privilege logs of other parties or non-parties that they are adopting and (b) Produce the non-privileged portions of any documents they are withholding on the basis of a claim of privilege. The Court resolves each of the motions for the reasons set forth on the record during the Conference. ACCORDINGLY, IT IS HEREBY ORDERED THAT: 1. Preska from Marjorie Peerce dated September 20, 2021. Fortino dated Septemdeferring ruling on 123 Letter Motion to Compel Full, Complete and Accurate Responses to Requests for Admissions addressed to Judge Loretta A. Fortino dated Septemgranting 117 Letter Motion for Conference on Motion to Compel Interrogatory Responses addressed to Judge Loretta A. Fortino dated Augdenying 115 Letter Motion for Conference addressed to Judge Loretta A.

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The Kansas Geological Survey does not guarantee this document to be free from errors or inaccuracies and disclaims any responsibility or liability for interpretations based on data used in the production of this document or decisions based thereon.ORDER CONCERNING DISCOVERY LETTER MOTIONS granting 108 Letter Motion for Conference addressed to Judge Loretta A. Placed on web Aporiginally published April 2010.

#Perian salviola brooks run mining pdf

This volume is available as an Acrobat PDF version (9.6 MB). This report on the Permian System in Kansas is 'a work in progress' and future multi-disciplinary studies of chrono- and sequence stratigraphy, climate history, structural aspects, sediment transport, and diagenesis will further enhance our understanding of the end of the Paleozoic in Kansas.Ĭover photo-The broad, flat surface in the center of the photo is the top of the Glenrock Limestone Member of the Red Eagle Limestone and the Carboniferous-Permian boundary at Tuttle Creek Lake Spillway in Pottawatomie County, Kansas. Economically these Permian rocks have been, and are, an important source of hydrocarbons, salt, gypsum, building stone, aggregate, and ground water. Fluctuations from shallow-marine to terrestrial environments associated with climate change as a result of the waning of Gondwana glaciers and latitudinal shifts are recorded in the Permian rocks of Kansas.

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Summaries of the lithofacies, thicknesses, depositional environments, and source areas of, and for, the rocks in each series provide a basis for inferring the history of the Permian in Kansas as currently understood. Currently accepted stratigraphic nomenclature for the Permian of Kansas recognizes the Wolfcampian, Leonardian, and Guadalupian Series, and the lithostratigraphic formations within each of these series reflect a wide spectrum of depositional environments. The upper boundary of the Permian is an erosional unconformity that is overlain by rocks of Cretaceous age. Rocks of Permian age in Kansas were first recognized in 1895, and by the early 21st century the internationally accepted boundary between the Permian and the Carboniferous (Pennsylvanian Subsystem) was recognized in Kansas at the base of the Bennett Shale Member of the Red Eagle Limestone.

Originally published in 2010 as Kansas Geological Survey Bulletin 257. Watney 3ġEmeritus Professor, Kansas State UniversityĢDepartment of Geology, Kansas State UniversityģKansas Geological Survey, The University of Kansas